Hydrolytic reactions of radon fluorides - Inorganic Chemistry (ACS

Hydrolytic reactions of radon fluorides. Lawrence Stein. Inorg. Chem. , 1984, 23 (22), pp 3670–3671. DOI: 10.1021/ic00190a051. Publication Date: Oct...
0 downloads 0 Views 279KB Size
Inorg. Chem. 1984, 23, 3670-3671

3670

'I/

It is instructive to examine the factor(s) responsible for the changes in kRI among the series of compounds examined. The variation of the rate constants with certain other kinetic and thermodynamic measures of the electron-transfer properties of alkyl iodides was explored. Each of the following gave approximate correlations: (a) the rates of inner-sphere reduction of RI by Co(CN)? l7 (or for Cr(15a11eN,)~+,'~which is not depicted but gives a quite comparable graph); (b) the enthalpy of formation of R.;I9 (c) the rate of iodine atom abstraction from R I by phenyl radicals;lg (d) the estimated standard reduction potentials of RLZ0 These correlations in a LFER sense are shown in Figure 2. Electron transfer from vC(CH~)~O toHR I appears to be governed by factors similar to those found for the several mechanisms (atom abstraction,21 electron transfer, dissociative reduction) by which RI is known to react. A finer distinctionZ2among the mechanisms cannot be made on the basis of the available data. Acknowledgment. This work was supported by the US. Department of Energy, Office of Basic Energy Sciences, Chemical Sciences Division, under Contract W-7405-ENG-82. Registry No. (H20)5CrCH(CH3)22+, 60764-48-9; (H20)5CrC(CHj)20H2+,32108-93-3; CH31, 74-88-4; CH,CH,I, 75-03-6; (CH,),CHI, 75-30-9; C-CSH~I,1556-18-9.

0

L ' I

0

log

2

I

(kg/kcel

3

1

I

0.7

0.0

0.9

1.0

I

-E0/ V

Figure 2. Attempted correlations of kRIwith parameters relating to the reductive dissociation of alkyl halides in terms of (A) log (kRICo/kMelCo), where kc" is the rate constant for CO(CN)~', (B) the enthalpy of formation of the alkyl radical, (C) log (kM"/kMdB), where km is the rate constant for iodine atom abstraction by phenyl radicals, and (D) Eo(estd)for the electrochemical reduction of the alkyl iodide.

Halpern, J. Ann. N.Y. Acad. Sci. 1974, 239, 2 . Samuels, G . J.; Espenson, J. H. Inorg. Chem. 1979, 18, 2587. Castelhano, A. L.; Griller, D. J . Am. Chem. SOC.1982, 104, 3655. Eberson, L. Acta Chem. Scand., Ser. B 1982, 836, 533. Halogen abstraction reactions by Et3Si follow the reactivity order CH3X 2 C2H5X< i-C3H7X: Chatgilialoglu, C.; Ingold, K. U.; Scaiano, J. C. J. Am. Chem. SOC.1982, 104, 5123. The absolute rate constants are, however, close to diffusion controlled in these systems, and the selectivity of the radical is diminished. Kochi, J. K.'Organometallic Mechanisms and Catalysis"; Academic Press: New York, 1978; pp 138-168. A detailed discussion of these mechanisms is presented in this reference.

kinetics, -d In [CrC(CH3),0H2+]/dt = kobsd,the expression for the experimental rate constant being kobsd =

kA

+ kHkRI[RIl/(kCr[Cr2+1 + kRI[RII)

(6)

The experimental data were analyzed by a nonlinear least-squares fit of the data to eq 6, with values of kA and kH set at values determined under these precise conditions (see Table I), and kcr taken to be 5.1 X lo7 M-' s-l, the same as in 0.15-1.0 M 2-PrOH at 22 f 2 OC.13 The resulting values of kRIare given in Table I. Alternatively, the equation can be recast into a linear form (eq 7) that permits graphical representation of the data, as illustrated in Figure 1. 1 kobsd

-

kA

1 -=-+ kH

kcr kHkRI

m2+1 [R1l

Contribution from the Chemistry Division, Argonne National Laboratory, Argonne, Illinois 60439

Hydrolytic Reactions of Radon Fluorides

(7)

Lawrence Stein

Products. The identification of CrRZ+as the product provides evidence for the reactions given above. The 2-propyl complex was isolated by ion-exchange chromatography and identified by its absorption spectrum and by its reactions with Br2 and Hg2+. In the latter case, kinetic data were also used to confirm its identity. Other complexes (CrCH32+, CrCH2CH32+)were identified by their visible/UV spectra and by the rates of their acidolysis reactions. Interpretation and Discussion The reactions shown are in complete accord with earlier studies of CrC(CH3)20H2+.They are supported in this case by the fit of the kinetic data to eq 6, as illustrated in Figure 1, and by the confirmation that CrRZ+is formed from a given RI. The reaction between .C(CH3)20H and R I is not without precedent, although the slowness of these reactions has precluded earlier kinetic measurements. For example, pulseradiolysis experiments16 set k < lo5 M-' s-] for the reduction of CH31by s C ( C H ~ ) ~ OatHpH 7. In contrast, the conjugate base of the radical, a more powerful reducing agent, reacts readily (CH31, k = 1.1 X lo8 M-' s-l ).I6 The method employed here is applicable to less reactive substrates, which is the case with all of these alkyl iodides (Table I).

Received May 1, I984

The chemistry of radon has been studied by radioactivetracer methods, since no stable isotopes of this element are known. It has been shown that radon reacts with fluorine,' halogen fluorides,2 and a number of oxidizing salt^.^,^ By comparing the properties of its products with known properties of krypton and xenon fluorides, it has been possible to deduce that radon forms a difluoride, RnF,, and derivatives of the difluoride, such as RnF+SbF6-, RnF+TaF6-, and RnF+BiF6-. The trace products are reduced to elemental radon by water in reactions that are analogous to those of KrF, and XeF, with water: KrF, + H 2 0 Kr + 1/202 + 2HF XeFz + H 2 0 Xe + 1/202 + 2HF

--

RnF,

(1) Fields, P. R.; Stein, L.; Zirin, M. H. J. Am. Chem. Soc. 1962,84,4164. ( 2 ) Stein, L. Science (Washington, D.C.) 1970, 168, 362. (3) Stein, L. Science (Washington, D.C.) 1972, 175, 1463. (4) Stein, L. Radiochim. Acta 1983, 32, 163. (5) Malm, J. G.; Appelman, E. H. At. Energy Reu. 1967, 7 (3), 3. (6) Bartlett, N.; Sladky, F. 0. In "Comprehensive Inorganic Chemistry"; Trotman-Dickenson, A. F., Ed.; Peraamon Press: Oxford, 1973: Vol. 1, pp 213-330.

(16) Brault, D.; Neta, P. J. Am. Chem. SOC.1981, 103, 2705.

0020-1669/84/1323-3670$01.50/0

+ H 2 0 +Rn + lI2O2+ 2HF

(In contrast, XeF4 and XeF, form stable solutions of X e O p )

Q

1984 American Chemical Societv

Inorg. Chem. 1984, 23, 3671-3673 The fluoride also coprecipitates from halogen fluoride solutions with XeF, and complexes of XeF, but not with XeF4.'sS Recently, Avrorin et ale9have reported the preparation of a higher fluoride of radon, either RnF4 or RnF6, and a water-soluble oxide, RnO,, in tracer experiments with isotope 222Rn. They hydrolyzed complex mixtures of products that had been obtained by heating radon, xenon, fluorine, bromine pentafluoride, and either sodium fluoride or nickel fluoride. Part of the radon volatilized on hydrolysis and part remained in the aqueous phase, suggesting the formation of Rn03. However, Avrorin et al. failed to closely examine the contents of the aqueous phase. In this note we report the results of experiments that we have carried out, using larger amounts of reagents and similar conditions, in an effort to confirm their findings. Experimental Section A Monel reactor (9.05-mL volume) attached to a Monel valve was loaded at room temperature with either NiF, (16.8-27.7 mmol) or NaF (39.3-42.9 mmol), cooled to -195 OC, and charged with BrFS (15.5-46.4 mmol), 2URn(49-221 pCi), xenon (0.544.57 mmol), and fluorine (54.7-57.1 mmol). Each mixture was heated at 250-265 OC for approximately 40 h. The excess fluorine was pumped off at -195 OC, and BrFSand uncomplexed XeFs were vacuum distilled from the reactor at 0 OC. (The XeF, product was complexes by NaF but not by NiF2). Products remaining in the reactor were then hydrolyzed with 8-15 mL of 0.10 M aqueous Xe03 solution at 0 OC. Radon in the hydrolysate was analyzed by measuring the y emissions of its daughters, 214Pband ,I4Bi, in equilibrium with their parent? The hydrolysate was centrifuged and the supernate transferred to a separate container; the radon was then analyzed in each fraction. The supernate was flushed with nitrogen for 5-10 min and the residue stirred with 10 mL of either water, 0.10 M XeO, solution, or 1 M KI solution; after 4 h, the analyses were repeated. To determine the behavior of radon in simpler mixtures, several experiments were carried out with only radon, fluorine, and NiF2or with only radon, fluorine, and NaF. Each mixture was heated at 335-350 OC for approximately 3 h, excess fluorine was pumped off at -195 OC, and the products were hydrolyzed as before. Results and Discussion In the experiments with quinary mixtures, we found that 70% or more of the radon initially bound as a nonvolatile fluoride was released as gas during the hydrolysis. However, the remainder was not in solution, as reported by Avrorin et al,, but was trapped in undissolved solid. After the centrifugation and purge with nitrogen, less than 0.2%of the radon remained in the liquid phase. Approximately 11-29% (corrected for decay) stayed in the NiF2 residue and 5-24% in the N a F residue during the course of these experiments. Stirring the solid with water, XeO, solution, or KI solution released a further amount of radon as gas but yielded no solution containing a soluble radon compound. Iodine was liberated when KI solution was added to the supernate, showing that X e 0 3 was not removed by the purge. In each experiment with radon, fluorine, and NiF,, a complex fluoride was formed [probably (RIIF+)~N~F~-, a noble-gas analogue of K2NiFa and Cs2NiF6]. The radon was found to be concentrated in the NiF2 powder at the end of the fluorination. In experiments with radon, fluorine, and NaF, the radon was found to be distributed throughout the reactor, suggesting that the simple fluoride RnF, was formed. During the hydrolysis of each product, part of the radon was released as gas and part trapped in the solid, as before. We conclude from this study that no higher fluoride or oxide of radon is formed in the procedure of Avrorin et al. but that, (7) Nefedov, V. D.; Toropova, M. A.; Avrorin, V. V.; Dudkin, B. N. Radiokhimiya 1971, 13, 916. (8) Avrorin, V. V.; Nefedov, V. D.; Toropova, M. A. Radiokhimiya 1974, 16, 261. (9) Avrorin V. V.; Krasikova, R. N.; Nefedov, V. D.; Toropova, M. A. Radiokhimiya 1981, 23, 879.

0020-1669/84/1323-3671$01.50/0

3671

instead, the radon is carried by solids. Other workers have also been misled by this phenomenon. In 1967, Haseltine and Moser'O reported the oxidation of radon in aqueous solutions with hydrogen peroxide, potassium permanganate, potassium persulfate, and other reagents, but Flohr and Appelman" showed that the radon had not been oxidized but merely trapped in suspended solids. Gusev and KirinI2later confirmed Flohr and Appelman's results, using barium as a carrier. Thus far, we have seen no evidence for the existence of radon compounds or ions in aqueous solutions. We have found that solutions of cationic radon can be prepared very readily, however, in nonaqueous solvents, such as hydrogen fluoride and halogen fluorides.,~~ Acknowledgment. This work was performed under the auspices of the Office of Energy Research, Division of Chemical Sciences, U S . Department of Energy, under Contract W-3 1-109-Eng-38. Registry No. RnF4, 18976-86-8; RnF6, 80948-45-4; RnO,, 80948-46-5; NiF,, 10028-18-9; NaF, 7681-49-4; BrF,, 7789-30-2; 222Rn,14859-67-7; Xe, 7440-63-3; F2, 7782-41-4. (10) Haseltine, M. W.; Moser, H. C. J . Am. Chem. SOC.1967, 89, 2498. (11) Flohr, K.; Appelman, E. H. J . Am. Chem. SOC.1968, 90, 3584. (12) Gusev, Yu. K.; Kirin, I. S. Radiokhimiya 1971, 13, 916.

Contribution from the Department of Chemistry and Laboratory for Molecular Structure and Bonding, Texas A&M University, College Station, Texas 77843

New Routes to the Preparation of the AquomoIybdenum(IV) Ion by Comproportionation Reactions F. Albert Cotton,* David 0. Marler, and Willi Schwotzer Received December 16, 1983

The existence of an aquomolybdenum(1V) ion was first demonstrated by Souchay and co-workers' in 1966. Beginning in 1975, efforts to establish the nuclearity of the aquo ion in solution produced proposals of both m o n ~ n u c l e a rand ~ - ~binuclear"-' structures. These conclusions were based on kinetic, electrochemical and cryoscopic measurements. However, the likelihood of a trinuclear structure of the sort shown in Figure l., e.g., [MO~(~~-O)(~-O)~(H,O)~]~+, was suggested by the fact that merely by addition under mild conditions of certain ligands to a solution of the aquo ion crystalline products were isolated in which an M O ~ ( ~ ~ - O ) ( ~ , -structure O ) ~ L ~ was found.8-'0 Direct evidence of the trinuclear character of the (1) Souchay, P.; Cadiot, M.;Duhameaux, M. C. R . Hebd. Seances Acad. Sci. 1966, 262, 1524. (2) Ramasami, T.; Taylor, R. S.; Sykes, A. G. J . Am. Chem. SOC.1975, 97, 5918. (3) Ojo, S. F.; Sasaki, Y.; Taylor, R. S.; Sykes, A. G. Inorg. Chem. 1976, 15, 1006.

(4) (5) (6) (7) (8) (9) (10)

Ardon, M.; Pernick. A. J . Am. Chem. SOC.1973, 95, 6871. Ardon, M.; Bino, A.; Yahaw, G. J . Am. Chem. SOC.1976, 98, 2338. Chalilpoyil, P.; Anson, F. C. Inorg. Chem. 1978, 17, 2418. Cramer, S. P.; Gray, H. B. J. Am. Chem. SOC.1979, 101, 2770. Bino, A.; Cotton, F. A.; Dori, Z . J . Am. Chem. SOC.1978, 100, 5252. Bino, A.; Cotton, F. A.; Dori, 2.J. Am. Chem. SOC.1979, 101, 3842. Schlemper, E. 0.; Hussian, M. S.; Murmann, R. K. Crysr. Srrucr. Commun. 1982, 11, 89.

0 1984 American Chemical Society